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Triassic) in Barreal Depocenter, San Juan Province, Argentina
Andean Geology ISSN: 0718-7092 ISSN: 0718-7106 [email protected] Servicio Nacional de Geología y Minería Chile Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Bodnar, Josefina; Iglesias, Ari; Colombi, Carina E.; Drovandi, Juan Martín Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Andean Geology, vol. 46, no. 3, 2019 Servicio Nacional de Geología y Minería, Chile Available in: https://www.redalyc.org/articulo.oa?id=173961656006 This work is licensed under Creative Commons Attribution 3.0 International. PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative Josefina Bodnar, et al. Stratigraphical, sedimentological and palaeofloristic characterization of ... Research article Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Caracterización estratigráfica, sedimentológica y paleoflorística del Grupo Sorocayense (Triásico) en el área de Barreal, provincia de San Juan, Argentina Josefina Bodnar *12 Redalyc: https://www.redalyc.org/articulo.oa? Universidad Nacional de La Plata, Argentina id=173961656006 [email protected] Ari Iglesias 23 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Carina E. Colombi 24 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Juan Martín Drovandi 24 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Received: 30 November 2017 Accepted: 30 October 2018 Published: 04 February 2019 Abstract: e northern area of Cuyo Basin (west-central Argentina) corresponds to the Rincón Blanco half-graben, whose filling is arranged into the Rincón Blanco and Sorocayense groups. -
M.Sc. Plant Science (Applicable to Students Admitted in 2009 Onwards)
M.Sc. Plant Science (Applicable to students admitted in 2009 onwards) (w.e.f. examination of 2009 onwards) M.Sc. I (Previous) Semester I Paper I - Microbiology (Bacteriology, Virology) and Microbial 100 Marks Biotechnology. Paper II - Mycology & Plant Pathology (Fungal Diseases) 100 Marks Paper III - Algology & Lichenology 100 Marks Paper IV - Bryology 100 Marks Practical - Based on Papers I to IV including 200 Marks Class and Field Work (Local excursion) 600 Marks Semester II Paper V - Pteridophytes 100 Marks Paper VI - Gymnosperms and Palaeobotany 100 Marks Paper VII - Angiosperms: Taxonomy and Economic Botany 100 Marks Paper VIII - Angiosperms: Histology, Anatomy, Embryology 100 Marks Practical - Based on Papers V to VIII 200 Marks - Class and Field Work (Local excursion) 600 Marks Students have to take all the eight papers. M.Sc. II (Final) Semester III Paper I - Cytology, Genetics and Cytogenetics 100 Marks Paper II - Plant Breeding and Biostatistics 100 Marks Paper III - Ecology, Environment and Soil Science 100 Marks Paper IV - Modern experimental techniques and computer application 100 Marks Practical - Based on Papers I to IV including 200 Marks - Class and field work/Laboratory visit 600 Marks Semester IV Paper V - Plant Physiology 100 Marks Paper VI - Cell Biology & Plant Biochemistry 100 Marks Paper VII - Biotechnology and Human welfare 100 Marks Paper VIII Elective - Project work (Review based on all Papers from 100 Marks Semester I to IV) Practical - Based on Papers V and VII 200 Marks (Incl. Biotech Lab visits & class work) 600 Marks Students have to take all the seven papers (a) The theory papers would have internal evaluation by the teaching/guest faculty as decided by the Coordinator in accordance with the nature and requirement of the subject and shall be notified to the students in the beginning of the semester. -
Reappraisal of the Genus Dicroidium Gothan from the Triassic Sediments of India
The Palaeobotanist 63(2014): 137–155 0031–0174/2014 Reappraisal of the genus Dicroidium Gothan from the Triassic sediments of India PANKAJ K. PAL1*, AMIT K. GHOSH2, RATAN KAR2, R.S. SINGH2, MANOBIKA SARKAR1 AND RESHMI CHATTERJEE2 1Department of Botany, UGC Centre of Advanced Study, University of Burdwan, Burdwan–713 104, West Bengal, India. 2Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India. *Corresponding author: [email protected] (Received 28 August, 2014; revised version accepted 25 September, 2014) ABSTRACT Pal PK, Ghosh AK, Kar R, Singh RS, Sarkar M & Chatterjee R 2014. Reappraisal of the genus Dicroidium Gothan from the Triassic sediments of India. The Palaeobotanist 63(2): 137–155. The genus Dicroidium Gothan, belonging to Corystospermaceae, is characterised by pinnately compound leaves with proximally forked primary rachis. The genus was earlier included under the genus Thinnfeldia Ettingshausen. Dicroidium is the most consistent macrofloral element in the Triassic strata of Southern Hemisphere. The present reassessment deals with the morphotaxonomy and stratigraphic significance of the species of Dicroidium in India. A critical review of the literature reveals that the specimens of Dicroidium described so far from India require reassessment, because same morphotypes have often been placed under different species names and sometimes dissimilar elements have been assigned to the same species. In view of this, a thorough analysis of Indian Dicroidium was undertaken based on fresh collections along with the species described earlier by previous workers. The present reappraisal reveals that the genus in the Triassic of Peninsular India is represented by eight species. These are D. hughesii (Feistmantel) Lele, D. -
Fundamentals of Palaeobotany Fundamentals of Palaeobotany
Fundamentals of Palaeobotany Fundamentals of Palaeobotany cuGU .叮 v FimditLU'φL-EjAA ρummmm 吋 eαymGfr 伊拉ddd仇側向iep M d、 況 O C O W Illustrations by the author uc削 ∞叩N Nn凹創 刊,叫MH h 咀 可 白 a aEE-- EEA First published in 1987 by Chapman αndHallLtd 11 New Fetter Lane, London EC4P 4EE Published in the USA by Chα~pman and H all 29 West 35th Street: New Yo地 NY 10001 。 1987 S. V. M秒len Softcover reprint of the hardcover 1st edition 1987 ISBN-13: 978-94-010-7916-7 e-ISBN-13: 978-94-009-3151-0 DO1: 10.1007/978-94-009-3151-0 All rights reserved. No part of this book may be reprinted, or reproduced or utilized in any form or by any electronic, mechanical or other means, now known or hereafter invented, including photocopying and recording, or in any information storage and retrieval system, without permission in writing from the publisher. British Library Cataloguing in Publication Data Mey凹, Sergei V. Fundamentals of palaeobotany. 1. Palaeobotany I. Title 11. Osnovy paleobotaniki. English 561 QE905 Library 01 Congress Catα loging in Publication Data Mey凹, Sergei Viktorovich. Fundamentals of palaeobotany. Bibliography: p. Includes index. 1. Paleobotany. I. Title. QE904.AIM45 561 8ι13000 Contents Foreword page xi Introduction xvii Acknowledgements xx Abbreviations xxi 1. Preservation 抄'pes αnd techniques of study of fossil plants 1 2. Principles of typology and of nomenclature of fossil plants 5 Parataxa and eutaxa S Taxa and characters 8 Peculiarity of the taxonomy and nomenclature of fossil plants 11 The binary (dual) system of fossil plants 12 The reasons for the inflation of generic na,mes 13 The species problem in palaeobotany lS The polytypic concept of the species 17 Assemblage-genera and assemblage-species 17 The cladistic methods 18 3. -
Diversity and Homologies of Corystosperm Seed-Bearing Structures from the Early Cretaceous of Mongolia Aã B,C D E F Gongle Shi , Peter R
Journal of Systematic Palaeontology ISSN: 1477-2019 (Print) 1478-0941 (Online) Journal homepage: https://www.tandfonline.com/loi/tjsp20 Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera To cite this article: Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera (2019) Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia, Journal of Systematic Palaeontology, 17:12, 997-1029, DOI: 10.1080/14772019.2018.1493547 To link to this article: https://doi.org/10.1080/14772019.2018.1493547 Published online: 14 Jan 2019. Submit your article to this journal Article views: 142 View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tjsp20 Journal of Systematic Palaeontology, 2019 Vol. 17, No. 12, 997–1029, http://dx.doi.org/10.1080/14772019.2018.1493547 Diversity and homologies of corystosperm seed-bearing structures from the Early Cretaceous of Mongolia aà b,c d e f Gongle Shi , Peter R. Crane , Patrick S. Herendeen , Niiden Ichinnorov , Masamichi Takahashi and Fabiany Herrerad aState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China; bOak Spring Garden -
Assessing the Record and Causes of Late Triassic Extinctions
Earth-Science Reviews 65 (2004) 103–139 www.elsevier.com/locate/earscirev Assessing the record and causes of Late Triassic extinctions L.H. Tannera,*, S.G. Lucasb, M.G. Chapmanc a Departments of Geography and Geoscience, Bloomsburg University, Bloomsburg, PA 17815, USA b New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104, USA c Astrogeology Team, U.S. Geological Survey, 2255 N. Gemini Rd., Flagstaff, AZ 86001, USA Abstract Accelerated biotic turnover during the Late Triassic has led to the perception of an end-Triassic mass extinction event, now regarded as one of the ‘‘big five’’ extinctions. Close examination of the fossil record reveals that many groups thought to be affected severely by this event, such as ammonoids, bivalves and conodonts, instead were in decline throughout the Late Triassic, and that other groups were relatively unaffected or subject to only regional effects. Explanations for the biotic turnover have included both gradualistic and catastrophic mechanisms. Regression during the Rhaetian, with consequent habitat loss, is compatible with the disappearance of some marine faunal groups, but may be regional, not global in scale, and cannot explain apparent synchronous decline in the terrestrial realm. Gradual, widespread aridification of the Pangaean supercontinent could explain a decline in terrestrial diversity during the Late Triassic. Although evidence for an impact precisely at the boundary is lacking, the presence of impact structures with Late Triassic ages suggests the possibility of bolide impact-induced environmental degradation prior to the end-Triassic. Widespread eruptions of flood basalts of the Central Atlantic Magmatic Province (CAMP) were synchronous with or slightly postdate the system boundary; emissions of CO2 and SO2 during these eruptions were substantial, but the contradictory evidence for the environmental effects of outgassing of these lavas remains to be resolved. -
Early Cretaceous Flora of India–A Review
The Palaeobotanist 65(2016): 209–245 0031–0174/2016 Early Cretaceous flora of India–A review A. RAJANIKANTH* AND CH. CHINNAPPA Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India. *Corresponding author: [email protected] (Received 23 September, 2015; revised version accepted 05 May, 2016) ABSTRACT Rajanikanth A & Chinnappa Ch 2016. Early Cretaceous flora of India–A review. The Palaeobotanist 65(2): 209–245. Earth’s terrestrial ecosystem during the early Cretaceous was marked by the dominance of naked seeded plants and appearance of flowering plants. Tectonic changes and evolutionary processes affected southern floras of the globe during this time. Review of Indian early Cretaceous flora distributed in peri and intra–cratonic basins signify homogenity of composition with regional variations. The flora composed of pteridophytes, pteridospermaleans, pentoxylaleans, bennettitaleans, ginkgoaleans, coniferaleans, taxaleans and taxa of uncertain affinity along with sporadic occurrence of flowering plants represent a unique Indian early Cretaceous flora. Similitude of basinal floras with marginal differences can be attributed to taphonomic limitations and taxonomic angularity. A perusal of available data brings out an opportunity for novelty in floral composition and variable associations dictated by prevailed environmental conditions. The eastern, western and central regions of India hold distinct litho units encompassing plant mega fossils represented by leaf, wood / axis, seed, fructification and associated marker forms. Remarkable tenacity of certain plant groups, which even found in modern flora and vulnerability of many taxa constitute a blend of extinct and extant. The appearance and extinction of certain taxa can be explained as a cumulative affect of evolutionary and climatic factors. -
PDF Publication
Palynology Results for the Wanship 7.5' Quadrangle, Summit and Morgan Counties, Utah by Carol L. Hotton1 and Zachary W. Anderson2 1 Department of Paleobiology, MRC-121, National Museum of Natural History, Smithsonian Institution, Washington DC 2 Utah Geological Survey, Salt Lake City, Utah Suggested citation: Hotton, C. L., and Anderson, Z.W., 2020, Palynology results for the Wanship 7.5' quadrangle, Summit and Morgan Counties, Utah: Utah Geological Survey Open-File Report 726, 7 p., https://doi.org/10.34191/OFR-726. OPEN-FILE REPORT 726 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 2020 Blank pages are intentional for printing purposes. INTRODUCTION This Open-File Report makes available raw analytical data from laboratory procedures completed to determine the age of rock samples collected during geologic mapping funded by the U.S. Geological Survey (USGS) National cooperative Geologic Mapping Program (STATEMAP) and the Utah Geological Survey (UGS). The reference listed in table 1 provides additional information such as the geologic setting of the samples in the context of the area in which they were collected. This report was pre-pared by Carol L. Hotton of the Smithsonian Institution in cooperation with the UGS. These data are highly technical in nature and proper interpretation requires expertise in recognition and interpretation of palynomorphs and their application to biostratigraphy. Table 1. Sample numbers, locations, and ages (see Anderson, in preparation). Easting Northing Interpreted Age Sample Map -
1 Relationships of Angiosperms To
Relationships of Angiosperms to 1 Other Seed Plants Seed plants are of fundamental importance both evolution- all gymnosperms (living and extinct) together are not arily and ecologically. They dominate terrestrial landscapes, monophyletic. Importantly, several fossil lineages, Cayto- and the seed has played a central role in agriculture and hu- niales, Bennettitales, Pentoxylales, and Glossopteridales man history. There are fi ve extant lineages of seed plants: (glossopterids), have been proposed as putative close rela- angiosperms, cycads, conifers, gnetophytes, and Ginkgo. tives of the angiosperms based on phylogenetic analyses These fi ve groups have usually been treated as distinct (e.g., Crane 1985; Rothwell and Serbet 1994; reviewed in phyla — Magnoliophyta (or Anthophyta), Cycadophyta, Doyle 2006, 2008, 2012; Friis et al. 2011). These fossil lin- Co ni fe ro phyta, Gnetophyta, and Ginkgophyta, respec- eages, sometimes referred to as the para-angiophytes, will tively. Cantino et al. (2007) used the following “rank- free” therefore be covered in more detail later in this chapter. An- names (see Chapter 12): Angiospermae, Cycadophyta, other fossil lineage, the corystosperms, has been proposed Coniferae, Gnetophyta, and Ginkgo. Of these, the angio- as a possible angiosperm ancestor as part of the “mostly sperms are by far the most diverse, with ~14,000 genera male hypothesis” (Frohlich and Parker 2000), but as re- and perhaps as many as 350,000 (The Plant List 2010) to viewed here, corystosperms usually do not appear as close 400,000 (Govaerts 2001) species. The conifers, with ap- angiosperm relatives in phylogenetic trees. proximately 70 genera and nearly 600 species, are the sec- The seed plants represent an ancient radiation, with ond largest group of living seed plants. -
Anatomy and Affinities of Permineralized Gymnospermous Trunks with Preserved Bark 2 from the Middle Triassic of Antarctica
Anatomy and affinities of permineralized gymnospermous trunks with preserved bark from the Middle Triassic of Antarctica Anne-Laure Decombeix, Edith L Taylor, Thomas N. Taylor To cite this version: Anne-Laure Decombeix, Edith L Taylor, Thomas N. Taylor. Anatomy and affinities of permineral- ized gymnospermous trunks with preserved bark from the Middle Triassic of Antarctica. Review of Palaeobotany and Palynology, Elsevier, 2010, 163, pp.26-34. 10.1016/j.revpalbo.2010.09.002. hal- 00656922 HAL Id: hal-00656922 https://hal.archives-ouvertes.fr/hal-00656922 Submitted on 5 Jan 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. NOTICE: This is the author’s version of a work accepted for publication by Elsevier. Changes resulting from the publishing process, including peer review, editing, corrections, structural formatting and other quality control mechanisms, may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Review of Palaeobotany and Palynology 163: 26-34, doi:10.1016/j.revpalbo.2010.09.002 1 Anatomy and affinities of permineralized gymnospermous trunks with preserved bark 2 from the Middle Triassic of Antarctica. -
An Advanced Peltasperm Permoxylocarpus Trojanus Naug
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Wulfenia Jahr/Year: 2010 Band/Volume: 17 Autor(en)/Author(s): Naugolnykh Serge V., Oskolski Alexei A. Artikel/Article: An advanced peltasperm Permoxylocarpus trojanus Naug. from the Lower Permian of the Urals (Russia): an ancient case of entomophily in gymnosperms? 29-43 © Landesmuseum für Kärnten; download www.landesmuseum.ktn.gv.at/wulfenia; www.biologiezentrum.at Wulfenia 17 (2010): 29 – 43 Mitteilungen des Kärntner Botanikzentrums Klagenfurt An advanced peltasperm Permoxylocarpus trojanus Naug. from the Lower Permian of the Urals (Russia): an ancient case of entomophily in gymnosperms? Serge V. Naugolnykh & Alexei A. Oskolski Summary: The evolutionarily advanced gymnosperm of peltaspermalean affi nity Permoxylocarpus trojanus Naug. from the Lower Permian deposits of the Urals (Russia) is described. Female reproductive organs of P. trojanus are spherical, semi-closed, peltate capsules with 15 –16 enclosed seeds. Both macromorphology and microstructure, including epidermal-cuticular characters and the anatomical structure of conducting tissues, are characterized. Sterile leaves of Praephylladoderma leptoderma Naug., provisionally belonging to the same parent plant, are also described. Some aspects of peltasperm evolution during the Late Palaeozoic – Early Mesozoic are briefl y summarized. The occurrence of enclosed ovuliferous organs (capsules) in some peltasperms, the structure of their pollen grains as well as some palaeoentomological evidences suggest the gradual shift from anemophily to entomophily in evolution of these gymnosperms. Keywords: peltasperms, evolution, Permian, seed-bearing organs, preangiosperms, fossil records, entomophily Pteridosperms sensu lato were widely distributed seed plants during the Late Palaeozoic. This very diverse group is commonly regarded as a grade rather than a well-supported clade. -
Triassic Floras of Antarctica: Plant Diversity and Distribution in High Paleolatitude Communities
PALAIOS, 2011, v. 26, p. 522–544 Research Article DOI: 10.2110/palo.2010.p10-122r TRIASSIC FLORAS OF ANTARCTICA: PLANT DIVERSITY AND DISTRIBUTION IN HIGH PALEOLATITUDE COMMUNITIES IGNACIO H. ESCAPA,1,2* EDITH L. TAYLOR,1 RUBE´ NCU´ NEO,2 BENJAMIN BOMFLEUR,1,3 JULIE BERGENE,1 RUDOLPH SERBET,1 and THOMAS N. TAYLOR 1 1Department of Ecology and Evolutionary Biology, and Natural History Museum and Biodiversity Institute, University of Kansas, Lawrence 66045-7534, USA, [email protected], [email protected], [email protected], [email protected], [email protected]; 2CONICET—Museo Paleontolo´gico Egidio Feruglio, Trelew, Chubut, 9100, Argentina, [email protected]; 3Forschungsstelle fu¨r Pala¨obotanik am Institut fu¨r Geologie und Pala¨ontologie, Westfa¨lische Wilhelms-Universita¨t Mu¨nster, Hindenburgplatz 57, D-48143 Mu¨nster, Germany, [email protected] ABSTRACT number of Antarctic plant fossils during his career. His collection—now at the University of Kansas—includes plants preserved as impressions Continental Triassic sequences in Antarctica are among the most and compressions, palynological samples, and silicified wood from continuous and best represented in Gondwana. Triassic fossil plants have numerous sites, including southern and northern Victoria Land (SVL, been collected sporadically from Antarctica since the beginning of the NVL) and the CTM. twentieth century, but our knowledge of the vegetation during this time Certainly one of the most significant contributions of Schopf’s has dramatically increased during the last three decades. Here we review fieldwork in Antarctica was the discovery of permineralized peat from the fossil record of Triassic plants as representatives of natural groups two sites in the CTM (Schopf, 1970, 1978).